Gondwana break-up related magmatism in the Falkland Islands
Jurassic dykes ( c . 182 Ma) are widespread across the Falkland Islands and exhibit considerable geochemical variability. Orthopyroxene-bearing NW–SE-oriented quartz-tholeiite dykes underwent fractional crystallization at >1 GPa, and major element constraints suggest that they were derived by mel...
Main Authors: | , , , |
---|---|
Format: | Dataset |
Language: | unknown |
Published: |
Geological Society of London
2016
|
Subjects: | |
Online Access: | https://dx.doi.org/10.6084/m9.figshare.3454094 https://geolsoc.figshare.com/articles/dataset/Gondwana_break-up_related_magmatism_in_the_Falkland_Islands/3454094 |
id |
ftdatacite:10.6084/m9.figshare.3454094 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.6084/m9.figshare.3454094 2023-05-15T13:34:28+02:00 Gondwana break-up related magmatism in the Falkland Islands M. J. Hole R. M. Ellam D. I. M. Macdonald S. P. Kelley 2016 https://dx.doi.org/10.6084/m9.figshare.3454094 https://geolsoc.figshare.com/articles/dataset/Gondwana_break-up_related_magmatism_in_the_Falkland_Islands/3454094 unknown Geological Society of London https://dx.doi.org/10.1144/jgs2015-027 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Geology FOS Earth and related environmental sciences dataset Dataset 2016 ftdatacite https://doi.org/10.6084/m9.figshare.3454094 https://doi.org/10.1144/jgs2015-027 2021-11-05T12:55:41Z Jurassic dykes ( c . 182 Ma) are widespread across the Falkland Islands and exhibit considerable geochemical variability. Orthopyroxene-bearing NW–SE-oriented quartz-tholeiite dykes underwent fractional crystallization at >1 GPa, and major element constraints suggest that they were derived by melting of a pyroxenite-rich source. They have εNd 182 in the range −6 to −11 and 87 Sr/ 86 Sr 182 >0.710 and therefore require an old lithospheric component in their source. A suite of basaltic-andesites and andesites exhibit geochemical compositions transitional between Ferrar and Karoo magma types, and are similar to those seen in the KwaZulu-Natal region of southern Africa and the Theron Mountains of Antarctica. Olivine-phyric intrusions equilibrated at <0.5 GPa, and have isotopic compositions (εNd 182 1.6–3.6 and 87 Sr/ 86 Sr 182 0.7036–0.7058) that require limited interaction with old continental lithosphere. A suite of plagioclase-phyric intrusions with 87 Sr/ 86 Sr 182 c . 0.7035 and εNd 182 c . +4, and low Th/Ta and La/Ta ratios ( c . 1 and c . 15, respectively) also largely escaped interaction with the lithosphere. These isotopically depleted intrusions were probably emplaced synchronously with Gondwana fragmentation and the formation of new oceanic lithosphere. Estimates of mantle potential temperature from olivine equilibration temperatures do not provide unequivocal evidence for the presence of a plume thermal anomaly beneath the Falkland Islands at 182 Ma. Dataset Antarc* Antarctica DataCite Metadata Store (German National Library of Science and Technology) Theron Mountains ENVELOPE(-28.068,-28.068,-79.044,-79.044) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Geology FOS Earth and related environmental sciences |
spellingShingle |
Geology FOS Earth and related environmental sciences M. J. Hole R. M. Ellam D. I. M. Macdonald S. P. Kelley Gondwana break-up related magmatism in the Falkland Islands |
topic_facet |
Geology FOS Earth and related environmental sciences |
description |
Jurassic dykes ( c . 182 Ma) are widespread across the Falkland Islands and exhibit considerable geochemical variability. Orthopyroxene-bearing NW–SE-oriented quartz-tholeiite dykes underwent fractional crystallization at >1 GPa, and major element constraints suggest that they were derived by melting of a pyroxenite-rich source. They have εNd 182 in the range −6 to −11 and 87 Sr/ 86 Sr 182 >0.710 and therefore require an old lithospheric component in their source. A suite of basaltic-andesites and andesites exhibit geochemical compositions transitional between Ferrar and Karoo magma types, and are similar to those seen in the KwaZulu-Natal region of southern Africa and the Theron Mountains of Antarctica. Olivine-phyric intrusions equilibrated at <0.5 GPa, and have isotopic compositions (εNd 182 1.6–3.6 and 87 Sr/ 86 Sr 182 0.7036–0.7058) that require limited interaction with old continental lithosphere. A suite of plagioclase-phyric intrusions with 87 Sr/ 86 Sr 182 c . 0.7035 and εNd 182 c . +4, and low Th/Ta and La/Ta ratios ( c . 1 and c . 15, respectively) also largely escaped interaction with the lithosphere. These isotopically depleted intrusions were probably emplaced synchronously with Gondwana fragmentation and the formation of new oceanic lithosphere. Estimates of mantle potential temperature from olivine equilibration temperatures do not provide unequivocal evidence for the presence of a plume thermal anomaly beneath the Falkland Islands at 182 Ma. |
format |
Dataset |
author |
M. J. Hole R. M. Ellam D. I. M. Macdonald S. P. Kelley |
author_facet |
M. J. Hole R. M. Ellam D. I. M. Macdonald S. P. Kelley |
author_sort |
M. J. Hole |
title |
Gondwana break-up related magmatism in the Falkland Islands |
title_short |
Gondwana break-up related magmatism in the Falkland Islands |
title_full |
Gondwana break-up related magmatism in the Falkland Islands |
title_fullStr |
Gondwana break-up related magmatism in the Falkland Islands |
title_full_unstemmed |
Gondwana break-up related magmatism in the Falkland Islands |
title_sort |
gondwana break-up related magmatism in the falkland islands |
publisher |
Geological Society of London |
publishDate |
2016 |
url |
https://dx.doi.org/10.6084/m9.figshare.3454094 https://geolsoc.figshare.com/articles/dataset/Gondwana_break-up_related_magmatism_in_the_Falkland_Islands/3454094 |
long_lat |
ENVELOPE(-28.068,-28.068,-79.044,-79.044) |
geographic |
Theron Mountains |
geographic_facet |
Theron Mountains |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
https://dx.doi.org/10.1144/jgs2015-027 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.3454094 https://doi.org/10.1144/jgs2015-027 |
_version_ |
1766053165057179648 |